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ANALYSIS OF SEISMOTECTONIC ACTIVITY OF IONIAN FAULT ZONE, ALBANIA
Abstract
The seismicity of Albania is primarily driven by the collision between the Adria microplate and the Albanian orogen. The Ionian fault zone, located in southwestern Albania, is characterized by NW-SE trending neotectonic thrust faults with oblique components. These faults are predominantly marked by NW extension and include pre-Pliocene overthrust faults subjected to pure compressive stress. Occasionally, these overthrust faults are intersected by NE-SW-oriented thrust faults. The Ionian overthrust fault zone extends over 100 km along the Ionian Sea coast, from Vlora to Konispol. This study analyzes the seismotectonic activity of the Ionian fault zone, using data from 166 earthquakes (4.5 = Ms = 6.6) recorded between 358 and 2024, including six events with magnitudes of 6.6. Notable earthquakes from the last century include the 1931 Qafe e Llogaras (Ms = 6.1) and the 1920 Tepelena (Ms = 6.4) events. A total of 3,837 earthquakes (0.1 = ML less than 5.2) have been recorded during the instrumental period (1970-2024). The most significant earthquake of the 21st century was the Bularati earthquake (ML = 5.2) on May 26, 2000. Seismic activity is concentrated along several fault segments, including Vlora-Qaf- e Llogaras-, Borsh-Kardhiq, and Pilur-Ku--Nivic--Tepelen-. Focal mechanism solutions for 54 earthquakes indicate predominantly reverse fault motion with a strike-slip component, reflecting compression along the SW-NE axis. The Ionian fault zone presents a significant seismic hazard, with potential future events up to Mmax 7.0. This study aims to enhance understanding of the region's seismotectonic framework.
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